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    Du Yifan, Zhu Xiaomin, Ye Lei, Gao Yuan, 2020. Features and Model of Mixed Sediments in Lower Submember of First Member of Shahejie Formation in Lixian Slope, Raoyang Sag. Earth Science, 45(10): 3759-3778. doi: 10.3799/dqkx.2020.215
    Citation: Du Yifan, Zhu Xiaomin, Ye Lei, Gao Yuan, 2020. Features and Model of Mixed Sediments in Lower Submember of First Member of Shahejie Formation in Lixian Slope, Raoyang Sag. Earth Science, 45(10): 3759-3778. doi: 10.3799/dqkx.2020.215

    Features and Model of Mixed Sediments in Lower Submember of First Member of Shahejie Formation in Lixian Slope, Raoyang Sag

    doi: 10.3799/dqkx.2020.215
    • Received Date: 2019-12-31
    • Publish Date: 2020-11-17
    • Not only are mixed rocks distributed in marine basins,but they are also distributed in a large number of hanging wall slope areas in rift sags and related to hydrocarbon accumulation closely. Mainly based on the core data and logging data of the Lixian slope,and the sedimentary characteristics and distribution of mixed beach-bars are studied through the core and thin section observation,grain size analysis,log facies analysis. Firstly,seismic data,pollen data,and trace element data were analyzed to restore the depositional environment controlling factors such as paleoclimate,paleo-provenance,paleogeomorphology,and paleo-water characteristics in the first member of Shahejie Formation. Then,the sedimentary model of the mixed beach-bars in the lower submember of the first member of Shahejie Formation in Lixian slope was systematically built. The results show that the beach-bar facies developed in the hanging wall slope area of Raoyang sag can be divided into siliciclastic beach-bars,carbonate beach-bars,and mixed beach-bars according to petrologic characteristics. Moreover,mixed beach-bars can be divided into component-mixed beach-bars and stratified-mixed beach-bars. The lithology of mixed beach-bar was mainly of calcareous sandstone,sandy oolitic limestone,and bioclastic limestone. The distribution of mixed beach-bar was controlled by factors such as paleoclimate,paleo-provenance,paleogeomorphology,and paleo-water characteristics. Therefore,different sedimentary patterns developed in different positions and different sedimentary stages on the slope. Stratified-mixed beach-bars and siliciclastic beach-bars were deposited in the near-shore ramp,and component-mixed beach-bars were deposited in the far-shore ramp. Carbonate beach-bars were mainly distributed on the far-shore low uplift.

       

    • 致谢: 感谢谈明轩博士、陈贺贺博士、张自力博士和李玲珑硕士给予本文的极富建设性的指导和大力帮助;感谢审稿专家和编委提出的珍贵意见建议!
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